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Coastal upwelling of the South Eastern Arabian Sea : ウィキペディア英語版 | Coastal upwelling of the South Eastern Arabian Sea Coastal upwelling of the South Eastern Arabian Sea (SEAS) is a typical eastern boundary upwelling system (EBUS) similar to the California, Bengulea, Canary Island and Peru-Chili systems. Unlike those four, the SEAS upwelling system needs to be explored in a much focused manner to clearly understand the chemical and biological responses associated with this coastal process. The coastal upwelling in the south-eastern Arabian Sea occurs seasonally. It begins in the mid Spring along the southern tip of India and as the season advances it spreads northward. It is not a uniform wind-driven upwelling system, but is driven by various factors. While at Cape Comorin it can be modeled as just wind-driven,〔 as the phenomena rises along the west coast of India, longshore wind stresses play an increasing role, as do atmospheric effects from the Bay of Bengal, such as Kelvin and Rossby waves. ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Coastal upwelling of the South Eastern Arabian Sea」の詳細全文を読む
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